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Estimating annual groundwater recharge coefficient for karst aquifers of the southern Apennines (Italy)

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Figure

Fig. 1. Map of the karst aquifers of the southern Apennines. Key to symbols: (A) limestone and dolomitic limestone units of the carbonateplatform series (Jurassic-Paleogene); (B) dolomitic units of the carbonate platform series (Trias-Liassic); (C) calcareous-marly units of theouter basin series (Trias-Paleogene); (D) pre-, syn- and late- orogenic molasses and terrigenous units (Cretaceous-Pliocene); (E) volcaniccenters (Pliocene-Quaternary); (F) alluvial and epiclastic units (Quaternary); (G) main basal springs of karst aquifers; (H) basal karst springsconsidered in the hydrological budget (a and b: Maretto and Torano; c: Salza Irpina; d and e: Serino; f: Baiardo; g: Cassano Irpino; h: Sanità;i: Avella; l: Ausino-Ausinetto); (I) hydrogeological boundary and identification number of the karst aquifers; (L) hydrogeological boundaryand identification number of the karst aquifers considered for the hydrological budget.
Fig. 2. Soil texture type, land use and geomorphological characteristics of the four sample karst aquifers.Loam, LS Loamy Sand.( (a) Soil texture frequency (SL Sandy (b) Land use frequency
Fig. 3. (a) Soil texture map. Common symbols: (i) hydrogeological boundary and identification number of the karst aquifers; (ii) hydrogeo-logical boundary and identification number of the sample karst aquifers
Fig. 4. Spatial distributions of rain gauge stations (a) and air temperature stations (b)
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